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Rates of Shoreline Progradation During the Last 1,700 Years at Beachmere,...
The morphology and chronostratigraphy of seven beach ridges at Beachmere, southeastern Queensland, Australia, provide a record of changes in shoreline accretion and relative sea... -
Seismic Stratigraphy and Sediment Distribution on the Wilkes Land and Terre...
Seismic reflection data show the existence of two major sedimentary basins along the continental margin of Wilkes Land and Terre Adélie, East Antarctica, that contain more than... -
Late Holocene sediment in Nara Inlet, central Great Barrier Reef platform,...
Nara Inlet in the Whitsunday Islands is a natural depocenter for clastic and carbonate sediment on the middle shelf of the central Great Barrier Reef (GBR) platform. Three... -
Environmental Management of Clastic Coastal Depositional Environments:...
Simple, conceptual geomorphic models can assist environmental managers in making informed decisions regarding management of the coast at continental and regional scales. This... -
Chemical, Biological and Hydrological Controls on the 14C Content of Cold...
Understanding the hydrology of cold seep environments is crucial to perform accurate estimates of fluid and chemical fluxes at sedimentary wedges. Shallow convection processes... -
Chemical Diversity in South-eastern Australian Saline Lakes II: Biotic Implications
This study explores how differences in ionic composition of south-eastern Australian saline lake waters, caused by path differentiation according to the Eugster-Jones-Hardie... -
Infaunal biodiversity and ecological function on a remote oceanic island:...
Understanding and predicting the processes determining biological assemblages and marine biodiversity is critical to managing and conserving marine ecosystems. Infauna are a... -
Pliocene-Pleistocene glaciomarine sedimentation in eastern Prydz Bay and...
Lithostratigraphy, grain sizes and down-hole logs of Site 1166 on the continental shelf, and Site 1167 on the upper slope, are analyzed to reconstruct glacial processes in... -
The Morphology of Barchan-shaped Sand Banks from Western Torres Strait,...
Large barchan shaped sand deposits have been observed in the north west of Torres Strait. These deposits share characteristics of both subaerial barchan dunes and subaqueous... -
A New High-resolution Depth Model for the Terre Adélie and George V Shelf...
Abstract: The Collaborative East Antarctic Marine Census (CEAMARC) surveys to the Terre Adélie and George V shelf and margin highlight the requirement for a revised high... -
Geophysical Variables as Predictors of Megabenthos Assemblages from the...
The question as to whether geophysical data from habitats can be used to predict the occurrence of benthic biodiversity is becoming more important with the increase in the use... -
Continental Shelf Record of the East Antarctic Ice Sheet Evolution:...
The late Quaternary ice sheet/ice shelf extent in the George V Basin (East Antarctica) has been reconstructed through analyses of Chirp sub-bottom profiles, integrated with... -
Climatic Variability in the Southwest Pacific during the Last Termination
The degree to which palaeoclimatic changes in the Southern Hemisphere co-varied with events in the high latitude Northern Hemisphere during the Last Termination is a contentious... -
Capricorn and northern Tasman Basins: Structure and Depositional Systems
The Bureau of Mineral Resources completed a major marine multi-channel seismic reflection survey (MCS) off southeast Queensland in December 1989. The research cruise, using RV... -
Late Neogene Ice Drainage Changes in Prydz Bay, East Antarctica and the...
During the late Neogene, the Lambert Glacier-Amery Ice Shelf drainage system flowed across Prydz Bay and showed several changes in flow pattern. In the Early Pliocene, the... -
Deep-sea bio-physical variables as surrogates for biological assemblages, an...
Deep sea environments occupy much of the sea floor, yet little is known about diversity patterns of biological assemblages from these environments. Physical mapping technologies... -
Geomorphological Evolution of Lord Howe Island and Carbonate Production at...
Lord Howe Island is a volcanic island, rising to over 800 m, draped with Late Quaternary submarine and subaerial carbonate sediments. The island and neighbouring islets lie... -
Biogeochemical Zones Within a Macrotidal, Dry-Tropical Fluvial-Marine...
The Fitzroy River delivers large amounts of nutrients and fine sediments to Keppel Bay (contiguous with the Great Barrier Reef Lagoon) during intermittent flow events. This... -
Facies Evolution of Holocene Estuaries and Deltas: A Large-sample...
Selected geomorphic features and sedimentary facies were mapped in 283 of Australia's wave- and tide-dominated estuaries and deltas to quantitatively evaluate established... -
Wind Generated Tool Marks Resembling Trace Fossils in a Shallow Estuarine Environment
A suite of tool marks were observed in the seaward section of a small estuary on the south coast of New South Wales, Australia. The marks were formed through wind dragging...